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Statements

Subject Item
dbr:Tasmantid_Seamount_Chain
rdf:type
geo:SpatialThing owl:Thing
rdfs:label
Catena sottomarina della Tasmania Tasmantid Seamount Chain
rdfs:comment
La catena sottomarina della Tasmania è una catena di montagne sottomarine lunga 2.000 km e situata nell'Oceano Pacifico meridionale. La catena consiste di oltre 16 picchi di vulcani estinti, molti dei quali si innalzano di oltre 4.000 m rispetto al fondale oceanico. È una delle due catene parallele di montagne sottomarine poste lungo la costa orientale dell'Australia; sia la catena sottomarina di Lord Howe che la catena della Tasmania si sviluppano in senso nord-sud attraverso il Mar dei Coralli e il Mar di Tasman. Le due catene hanno longitudine rispettivamente 159°E e 156°E. The Tasmantid Seamount Chain is a 2,000 km (1,200 mi) long chain of seamounts in the South Pacific Ocean. The chain consists of over 16 extinct volcanic peaks, many rising more than 4,000 m (13,000 ft) from the seabed. It is one of the two parallel seamount chains alongside the East Coast of Australia; the Lord Howe and Tasmantid seamount chains both run north-south through parts of the Coral Sea and Tasman Sea. These chains have longitudes of approximately 159°E and 156°E respectively.
dbp:name
Tasmantid Seamount Chain
geo:lat
-31.0
geo:long
156.0
foaf:depiction
n15:Zealandia,_topographic_map.jpg
dcterms:subject
dbc:Guyots dbc:Landforms_of_the_Coral_Sea dbc:Volcanoes_of_Australia dbc:Hotspot_tracks dbc:Seamounts_of_the_Tasman_Sea dbc:Tasman_Sea dbc:Volcanoes_of_the_Tasman_Sea dbc:Seamount_chains dbc:Miocene_volcanoes dbc:Seamounts_of_the_Pacific_Ocean
dbo:wikiPageID
53254105
dbo:wikiPageRevisionID
1109548614
dbo:wikiPageWikiLink
dbc:Seamounts_of_the_Pacific_Ocean dbr:South_Pacific_Ocean dbr:Moreton_Seamount dbr:Tasmantid_hotspot dbr:Seabed dbr:Tasman_Sea dbr:Coral_Sea dbr:156th_meridian_east dbr:Extinct_volcano dbr:Brisbane_Guyot dbr:Cato_Reef dbr:Indo-Australian_Plate dbr:Barcoo_Bank dbc:Volcanoes_of_Australia dbc:Hotspot_tracks dbc:Guyots dbr:Lord_Howe_Seamount_Chain dbc:Landforms_of_the_Coral_Sea dbr:Seamount_chain dbr:Australia dbr:Tasmanian_Seamounts dbr:Queensland_Guyot dbc:Seamounts_of_the_Tasman_Sea dbr:East_Coast_of_Australia dbc:Volcanoes_of_the_Tasman_Sea dbr:Derwent_Hunter_Guyot dbr:Stradbroke_Seamount dbc:Seamount_chains dbr:Recorder_Guyot dbc:Tasman_Sea dbr:Fraser_Seamount dbc:Miocene_volcanoes dbr:159th_meridian_east dbr:Taupo_Bank dbr:Seamounts dbr:Zealandia dbr:Longitude dbr:Kenn_Reef dbr:Gascoyne_Seamount dbr:Britannia_Guyots dbr:Wreck_Reefs
owl:sameAs
wikidata:Q29025817 yago-res:Tasmantid_Seamount_Chain n17:2gxmL dbpedia-it:Catena_sottomarina_della_Tasmania
dbp:wikiPageUsesTemplate
dbt:Reflist dbt:Coord dbt:Infobox_seamount dbt:Convert dbt:Distinguish dbt:Short_description
dbo:thumbnail
n15:Zealandia,_topographic_map.jpg?width=300
dbp:imageCaption
Topographic map of Zealandia that includes the unlabelled Tasmantid Seamount Chain off the east of Australia extending from the Coral Sea southwards into the Tasman Sea.
dbp:location
Coral and Tasman seas
dbp:mapCaption
Tasmantid Seamount Chain
dbp:mapSize
250
dbp:type
dbr:Seamount_chain
georss:point
-31.0 156.0
dbo:abstract
The Tasmantid Seamount Chain is a 2,000 km (1,200 mi) long chain of seamounts in the South Pacific Ocean. The chain consists of over 16 extinct volcanic peaks, many rising more than 4,000 m (13,000 ft) from the seabed. It is one of the two parallel seamount chains alongside the East Coast of Australia; the Lord Howe and Tasmantid seamount chains both run north-south through parts of the Coral Sea and Tasman Sea. These chains have longitudes of approximately 159°E and 156°E respectively. Like its neighbour, the Tasmantid Seamount Chain has resulted from the Indo-Australian Plate moving northward over a stationary hotspot. It ranges in age from 40 to 6 million years old. Alternative names for the Tasmantid Seamount Chain include the Tasmantid Seamounts, Tasman Seamounts, Tasman Seamount Chain, Tasmantide Volcanoes or simply the Tasmantids. La catena sottomarina della Tasmania è una catena di montagne sottomarine lunga 2.000 km e situata nell'Oceano Pacifico meridionale. La catena consiste di oltre 16 picchi di vulcani estinti, molti dei quali si innalzano di oltre 4.000 m rispetto al fondale oceanico. È una delle due catene parallele di montagne sottomarine poste lungo la costa orientale dell'Australia; sia la catena sottomarina di Lord Howe che la catena della Tasmania si sviluppano in senso nord-sud attraverso il Mar dei Coralli e il Mar di Tasman. Le due catene hanno longitudine rispettivamente 159°E e 156°E. Coma la sua vicina, la catena sottomarina della Tasmania è stata generata dalla placca indo-australiana in movimento verso nord sopra il punto caldo della Tasmania. L'età delle montagne sottomarine che ne fanno parte è compresa tra 40 e 6 milioni di anni.
prov:wasDerivedFrom
wikipedia-en:Tasmantid_Seamount_Chain?oldid=1109548614&ns=0
dbo:wikiPageLength
9077
foaf:isPrimaryTopicOf
wikipedia-en:Tasmantid_Seamount_Chain
geo:geometry
POINT(156 -31)